Preprints
https://doi.org/10.5194/bg-2022-215
https://doi.org/10.5194/bg-2022-215
 
07 Nov 2022
07 Nov 2022
Status: this preprint is currently under review for the journal BG.

Ideas and perspectives: Alleviation of functional limitation by soil organisms is key to climate feedbacks from northern soils

Gesche Blume-Werry1, Jonatan Klaminder1, Eveline J. Krab1,2, and Sylvain Monteux3 Gesche Blume-Werry et al.
  • 1Climate Impacts Research Centre, Department of Ecology and Environmental Science, Umeå University, Sweden
  • 2Swedish University of Agricultural Sciences, Department of Soil and Environment, Sweden
  • 3Department of Environmental Science, Stockholm University, Sweden

Abstract. Northern soils play an important role in Earth’s climate system as they store large amounts of carbon that, if released, could strongly increase greenhouse gas levels in our atmosphere. Most research to date has focused on how the turnover of organic matter in these soils is regulated by abiotic factors and few studies have considered the potential role of biotic regulation. Here, we claim that soil organisms’ presence or absence is key to understanding and predicting future climate feedbacks from northern soils. We propose that the arrival of soil organisms with currently ‘missing traits’, i.e., properties that the present community does not have, can alleviate functional limitation and result in greatly enhanced decomposition rates, in parity with effects predicted due to increasing temperatures. We base this argument on a series of emerging evidence suggesting that the dispersal of until-then absent micro-, meso- and macro-organisms (i.e., microbes and invertebrate soil fauna) into new regions and newly-thawed soil layers can drastically affect soil functioning. These new observations make us question the current view that neglects organism driven ‘alleviation effects’ when predicting the future feedbacks between northern ecosystems and our planets’ climate. We therefore advocate for an updated framework in which soil biota and their traits become essential when predicting the fate of soil functions in warming northern ecosystems.

Gesche Blume-Werry et al.

Status: open (until 03 Jan 2023)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Gesche Blume-Werry et al.

Gesche Blume-Werry et al.

Viewed

Total article views: 290 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
236 50 4 290 2 4
  • HTML: 236
  • PDF: 50
  • XML: 4
  • Total: 290
  • BibTeX: 2
  • EndNote: 4
Views and downloads (calculated since 07 Nov 2022)
Cumulative views and downloads (calculated since 07 Nov 2022)

Viewed (geographical distribution)

Total article views: 306 (including HTML, PDF, and XML) Thereof 306 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 09 Dec 2022
Download
Short summary
Northern soils store a lot of carbon. Most research has focused on how this carbon storage is regulated by cold temperatures. However, it is soil organisms, from minute bacteria to large earthworms, that decompose the organic material. Novel soil organisms from further south could increase decomposition rates more than climate change does and lead to carbon losses. We therefore advocate for including soil organisms when predicting the fate of soil functions in warming northern ecosystems.
Altmetrics